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生态学杂志 ›› 2026, Vol. 45 ›› Issue (8): 2522-2530.doi: 10.13292/j.1000-4890.202608.029

• 研究论文 • 上一篇    下一篇

植食性土壤动物对我国东部典型森林细根生产量的影响

仇叶童1,龙福强2,张棋渲1,郑敬曦1,王秀伟1*,孙涛2   

  1. 1东北林业大学林学院, 哈尔滨 150040; 2森林生态与保育重点实验室(中国科学院), 中国科学院沈阳应用生态研究所, 沈阳 110016)

  • 出版日期:2026-08-10 发布日期:2026-08-13

The impact of herbivorous soil animals on fine root production of typical forests in eastern China.

QIU Yetong1, LONG Fuqiang2, ZHANG Qixuan1, ZHENG Jingxi1, WANG Xiuwei1*, SUN Tao2   

  1. (1School of Forestry, Northeast Forestry University, Harbin 150040, China; 2CAS Key Laboratory of Forest Ecology and Silviculture, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China).

  • Online:2026-08-10 Published:2026-08-13

摘要: 细根作为陆地生态系统碳循环的核心组分,其生产量受环境与生物因子共同调控。植食性土壤动物是影响细根周转的重要因子。为了揭示大尺度地理格局下植食性土壤动物对植物细根生产量的影响机制,本研究在中国东部从南到北的17个天然次生林中布设研究样地(纬度18°36′N—53°26′N),并通过喷洒杀虫剂来控制植食性土壤动物的取食。处理一年后,在0~20 cm深度的土层中收集细根并采用根序法对其进行分级后测定生产量,从而探究植食性土壤动物对吸收根(AFR)与运输根(TFR)产量的影响。结果表明:(1)自然条件下,AFR与TFR产量均呈现显著的北低南高趋势,热带及亚热带地区产量显著高于温带及寒温带区域。其中,热带样地的AFR产量为寒温带(78~94 g·m-2)的1.5~2.1倍,TFR产量是寒温带(138~150 g·m-2)的3~4倍。中亚热带部分样地因微环境差异,产量低于同气候带邻近区域。(2)排除植食性土壤动物后,约半数样地的AFR和TFR产量显著增加(P<0.05),但不同纬度带响应强度差异显著:低纬度热带亚热带地区AFR产量增幅达20%~25%,TFR产量增幅25%~30%,部分亚热带样地吸收根产量跃居邻近纬度高位;高纬度寒温带至温带地区AFR产量增幅仅10%~15%,寒温带样地成为产量低值区,且无显著地理梯度。双因素方差分析表明,处理效应与纬度带存在显著交互作用(P<0.05),低纬度地区土壤动物对细根产量的调控效应更强。(3)细根产量与纬度呈极显著负相关,与年均温、年降水量呈极显著正相关,证实水热条件是主导地理分异的基础因子。植食性土壤动物的调控效应呈现纬度依赖性:低纬度地区通过摄食压力诱导植物补偿性生长,高纬度低温环境则抑制土壤动物活性,使其影响被气候因子掩盖。本研究为进一步探讨土壤生态系统中植食性动物与细根生产量的关系提供了重要参考,同时对认识森林生态系统能量流动和物质循环的关系具有重要的理论意义。


关键词: 细根生产量, 植食性土壤动物, 根序分级法, 内生长法, 天然次生林

Abstract: As a key component of carbon cycling in terrestrial ecosystems, the production of fine roots is regulated by both environmental and biological factors. Herbivorous soil animals are an important factor influencing fine root turnover. To elucidate the mechanisms by which herbivorous soil animals influence fine root production across broad geographical gradients, we established 17 plots in natural secondary forests spanning a latitudinal range of 18°36′N-53°26′N in eastern China. We manipulated herbivorous soil animal activity by applying insecticides to control their feeding on roots. Following one-year treatment, fine roots were collected from the 0-20 cm soil layer, classified using the root order classification approach, and their production was quantified to examine differential responses of absorptive fine root (AFR) and transport fine root (TFR) yields to herbivory disturbance. The results showed that: (1) under natural conditions, both AFR and TFR production exhibited a significant increasing trend from north to south sites, with yields in tropical and subtropical regions being significantly higher than those in temperate and cold-temperate regions. Specifically, AFR production in tropical forests was 1.5-2.1 times of that in cold-temperate plots (78-94 g·m-2), and TFR production was 3-4 times of that in cold-temperate plots (138-150 g·m-2). Some mid-subtropical plots had lower yields than adjacent areas in the same climatic zone due to micro-environmental differences. (2) After excluding herbivorous soil animals, AFR and TFR production significantly increased  in half of the plots, but the magnitude of response differed significantly across latitude zones. AFR production increased by 20%-25% and TFR production by 25%-30% in low-latitude tropical and subtropical regions, with AFR yields in some subtropical plots being the highest among adjacent latitudes after treatment. AFR production increased by only 10%-15% in high-latitude cold-temperate to temperate regions, with cold-temperate plots becoming low-yield areas and showing no significant geographical gradient. Two-way ANOVA Showed that there was a significant interaction between treatment effects and latitude zones (P<0.05), with a stronger regulatory effect of soil animals on fine root production in low-latitude regions. (3) Fine root production was highly significantly negatively correlated with latitude and significantly positively correlated with mean annual temperature and annual precipitation, confirming that hydrothermal condition is the fundamental driver of geographical differentiation of fine root production. The regulatory effect of herbivorous soil animals showed latitudinal dependency. Low-latitude regions induced plant compensatory growth through feeding pressure, while high-latitude low-temperature environments inhibited soil animal activity, masking their effects by climatic factors. This study provides an important reference for further exploring the relationship between herbivorous soil animals and fine root production in forests, and has important theoretical significance for understanding the relationship between energy flow and material cycling in forest ecosystems.


Key words: fine root production, herbivorous soil animal, root order classification method, ingrowth method, natural secondary forest